1887
Volume 23, Issue 1-2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Geological understanding of the Eastern Goldfields has been limited in the past by poor outcrop owing to regolith and surficial cover. The economic importance of the greenstone belts relative to gneiss and granitoids, has led to geological maps and models concentrating on the geology and geological evolution of the greenstone belts. The regional aeromagnetic and gravity data are used to derive models for the whole area, and therefore also to subdivide the nongreenstone rock. Interpretation of these regional geophysical data sets indicates the presence of features which are tens to hundreds of kilometres long. They include gneiss-granite domains, gneiss-granite domes, greenstone terranes and large bodies of granite. Recent more detailed surveys acquired under the National Geoscience Mapping Accord provide better resolution of the internal structure of these domains and enhance characteristic anomaly patterns used to discriminate between domains. Greenstone-belt deformation has been influenced by the shape of adjacent gneiss-granite domains, granites and lineaments. The geophysical models developed provide a valuable framework in which to assemble a wide variety of geological, geochemical, and geophysical information. It is through the generation of comprehensive regional models of the geology that effective exploration of areas of poor outcrop will be developed.

Loading

Article metrics loading...

/content/journals/10.1071/EG992429
1992-03-01
2026-01-13
Loading full text...

Full text loading...

References

  1. Barley, M. E., Eisenlohr, B. N., Groves, D. I., Perring, C. S., and Vearncombe, J. R. (1989). ‘Late Archaean convergent margin tectonics and gold mineralisation: a new look at the Norseman-Wiluna Belt, Western Australia.’ Geology56, 229–225.
  2. Gee, R. D. (1979). ‘Structure and tectonic style of the West Australian Shield’. Tectonophysics58, 327–369.
  3. Hill, R. E. T., and Gole, M. J. (1990). ‘Nickel Sulphide Deposits of the Yilgarn Craton.’ In Geology of the Mineral Deposits of Australia and Papua New Guinea, Ed. F. E. Hughes. Australian Institute of Mining and Metallurgy, Melbourne, 557–559.
  4. Williams, P. R., and Whitaker, A. J. (in press). ‘Gneiss domes and extensional deformation in the Archaean Eastern Goldfields Province, Western Australia’. Ore Geology Reviews.
  5. Whitaker, A. J. (1989). ‘A geophysical model for the Precambrian of the Albany 1:1M Sheet, Western Australia, and its relevance to economic geology.’ Explor. Geophys.20, 195–199.
/content/journals/10.1071/EG992429
Loading
  • Article Type: Research Article
Keyword(s): Archaean; Eastern Goldfields Province; gravity; greenstones; magnetics; Yilgarn Block

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error